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Revisiting the Palaeolithic site of Kulbulak (Uzbekistan): First results from luminescence dating

机译:重新探访库尔布拉克(乌兹别克斯坦)的旧石器遗址:发光测年的第一个结果

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Kulbulak has been considered as a key site for the Palaeolithic archaeology in Central Asia. Its significance, however, is under debate. Our analysis of the lithics provides no evidence for a Lower Palaeolithic industry, and challenges the existence of the "Denticulate Mousterian" as a particular Middle Palaeolithic facies in Western Central Asia. One limitation to interpreting the record preserved at Kulbulak, has been the lack of a chronological framework. In this paper, we report on the first age results that we have obtained for the sedimentary sequence using luminescence signals from potassium feldspar. We applied a conventional approach, which consists of stimulating single-aliquots of feldspar with infrared at 50 ℃ after a preheat of 250 ℃ for 60 s. The characteristics of this luminescence signal are documented, and it is shown to suffer from anomalous fading. The fading rates measured in the laboratory are used for correcting the ages. In general, the fading-corrected ages are stratigraphically consistent and agree with the archaeological evidence; they bracket the upper 6 m of the sequence in between 39 ± 4 ka and 82 ± 9 ka. These are among the first dates for human occupation during the Upper and Middle Palaeolithic in the region, but should be interpreted with caution owing to the limitations of the fading-correction model.
机译:库尔布拉克(Kulbulak)被认为是中亚旧石器时代考古的重要地点。但是,其意义还在争论中。我们对岩性的分析没有为下旧石器时代的工业提供任何证据,并且挑战了“齿状穆斯特”的存在,因为它是中亚西部特定的中古旧石器相。解释在库尔布拉克(Kulbulak)保存的记录的一个限制是缺乏按时间顺序排列的框架。在本文中,我们报告了使用钾长石的发光信号获得的沉积序列的第一年龄结果。我们采用了一种常规方法,该方法包括在250℃预热60 s后,在50℃下用红外线刺激长石的等分试样。该发光信号的特征已被记录,并且显示出异常衰落。实验室测量的衰落率用于校正年龄。通常,经过衰落校正的年龄在地层上是一致的,并且与考古证据相符。它们将序列的高6 m括在39±4 ka和82±9 ka之间。这些是该地区上,中部旧石器时代人类占领的最初日期,但由于衰落校正模型的局限性,应谨慎解释。

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  • 来源
    《Quaternary International》 |2014年第4期|180-189|共10页
  • 作者单位

    Laboratory of Mineralogy and Petrology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium,Regional Geomorphology and Geoarchaeology, Department of Geography, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium;

    F.R.S.-FNRS, Department of Prehistory, Liege University, Place du 20-Aout 7, 4000 Liege, Belgium;

    Regional Geomorphology and Geoarchaeology, Department of Geography, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium;

    Laboratory of Mineralogy and Petrology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium;

    Institute of Archaeology and Ethnography, Russian Academy of Sciences (Siberian Branch), Lavrentieva prosp. 17, 630090 Novosibirsk, Russia;

    Institute of Archaeology and Ethnography, Russian Academy of Sciences (Siberian Branch), Lavrentieva prosp. 17, 630090 Novosibirsk, Russia;

    Institute of Archaeology, Uzbek Academy of Sciences, Tashkent, Uzbekistan;

    Laboratory of Mineralogy and Petrology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium;

    Laboratory of Mineralogy and Petrology, Department of Geology and Soil Science, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium;

    Nordic Laboratory for Luminescence Dating, Department of Geoscience, Aarhus University, DTU Ris(e) Campus, DK-4000 Roskilde, Denmark,Technical University of Denmark, Center for Nuclear Technologies, DTU Ris(e) Campus, Building 201, Frederiksborgvej 399, DK-4000 Roskilde, Denmark;

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  • 入库时间 2022-08-18 03:35:27

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